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ANALYSES OF ERRORS IN MEDIUM-TERM NUMERICAL FORECAST PRODUCTS FOR THE SUBTROPICAL HIGH 1998

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  • By statistic and dynamic analyses, we have come to the following conclusions: (1) The ECMWF medium-term numerical forecast can forecast medium-term activity of subtropical high, and the accuracy rate of forecast cannot have large improvement by translational corrections. (2) The important cause for the ECMWF medium-term numerical forecast to have errors in 1998 is that the astronomical tide is not included in the model. (3) Two indexes are found from which it can be judged that ECMWF medium-term numerical forecast will have errors if the astronomical tide is ignored in the model : ① When the 54.7° line under the moon of the nodical month astronomical singularities coincides with the trough-line of the subtropical jet flow from 50°E to 150°E on the 500 hPa level at 2000 L.T. of the same day, and is approximately vertical (α>60°) with the isotherm, then the day 0 –C 2 days after the appearance of the nodical month astronomical singularities is defined as the initial day. Then in three successive days after the initial day, ECMWF medium-term numerical forecast of the northern latitude of the 588 line at 120 °E will have continuous errors as large as two latitudes (7/9). Otherwise, it won't have continuous errors (13/13). ② Otherwise, if the 54.7 ° line is in the range of a low pressure between two high pressures, then there is a dispersive error on the day of the nodical month astronomical singularities (5/7). There is not any error (6/6) otherwise.
  • [1] REN Zhen-qiu, ZHANG Su-qin. Astronomical singular points and anomalously southward subtropical high inthe prime summer of 1980 [J]. Meteorological Monthly, 1981, (3): 4-5.
    [2] WANG Xing-rong. Relationship between the astronomical tides and cold-wave weather under differenttopographic conditions [J]. Acta Meteorologica Sinica, 1990, 48: 239-241.
    [3] WANG Xing-rong, YAN Xue-feng. Relationship between the Mei-yu, subtropical high activity andanomalistic month [J]. Chinese Journal of Atmospheric Sciences, 1995, 19: 636-640.
    [4] WANG Xin-rong, SHI Zhen-ling, YAN Xue-feng, et al. Relationship between the subtropical high activityand solar and lunar circulation [J]. Journal of Tropical Meteorology, 1997, 13: 92-96.
    [5] WANG Xing-rong, WANG Zhong-xing, SHI Chun-er. On the non-conservation of wet potential vortex in theatmospheric movement [J]. Acta Meteorologica Sinica, 1998, 13(2): 136-141.
    [6] WANG Xing-rong, WU Ke-jun. Discussions of some issues on wet aerodynamics [J]. Acta MeteorologicaSinica, 1995, 15(1): 9-17.
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WANG Xing-rong, YAO Ye-qing, SHANG Yu, et al. ANALYSES OF ERRORS IN MEDIUM-TERM NUMERICAL FORECAST PRODUCTS FOR THE SUBTROPICAL HIGH 1998 [J]. Journal of Tropical Meteorology, 2003, 9(1): 105-112.
WANG Xing-rong, YAO Ye-qing, SHANG Yu, et al. ANALYSES OF ERRORS IN MEDIUM-TERM NUMERICAL FORECAST PRODUCTS FOR THE SUBTROPICAL HIGH 1998 [J]. Journal of Tropical Meteorology, 2003, 9(1): 105-112.
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ANALYSES OF ERRORS IN MEDIUM-TERM NUMERICAL FORECAST PRODUCTS FOR THE SUBTROPICAL HIGH 1998

Abstract: By statistic and dynamic analyses, we have come to the following conclusions: (1) The ECMWF medium-term numerical forecast can forecast medium-term activity of subtropical high, and the accuracy rate of forecast cannot have large improvement by translational corrections. (2) The important cause for the ECMWF medium-term numerical forecast to have errors in 1998 is that the astronomical tide is not included in the model. (3) Two indexes are found from which it can be judged that ECMWF medium-term numerical forecast will have errors if the astronomical tide is ignored in the model : ① When the 54.7° line under the moon of the nodical month astronomical singularities coincides with the trough-line of the subtropical jet flow from 50°E to 150°E on the 500 hPa level at 2000 L.T. of the same day, and is approximately vertical (α>60°) with the isotherm, then the day 0 –C 2 days after the appearance of the nodical month astronomical singularities is defined as the initial day. Then in three successive days after the initial day, ECMWF medium-term numerical forecast of the northern latitude of the 588 line at 120 °E will have continuous errors as large as two latitudes (7/9). Otherwise, it won't have continuous errors (13/13). ② Otherwise, if the 54.7 ° line is in the range of a low pressure between two high pressures, then there is a dispersive error on the day of the nodical month astronomical singularities (5/7). There is not any error (6/6) otherwise.

WANG Xing-rong, YAO Ye-qing, SHANG Yu, et al. ANALYSES OF ERRORS IN MEDIUM-TERM NUMERICAL FORECAST PRODUCTS FOR THE SUBTROPICAL HIGH 1998 [J]. Journal of Tropical Meteorology, 2003, 9(1): 105-112.
Citation: WANG Xing-rong, YAO Ye-qing, SHANG Yu, et al. ANALYSES OF ERRORS IN MEDIUM-TERM NUMERICAL FORECAST PRODUCTS FOR THE SUBTROPICAL HIGH 1998 [J]. Journal of Tropical Meteorology, 2003, 9(1): 105-112.
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